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- Canfield_ocean abstract "The Canfield Ocean model refers to the Ocean composition theorized by geologist Donald Canfield. In a seminal paper in Nature in 1998, Canfield argued that the Ocean had become partially anoxic and sulfidic during Proterozoic.Peter Ward studies the effects of ocean hypoxia(anoxic) and sulfidic oceans and climate change. He found warming of the ocean caused by a rise of carbon dioxide levels to about 1000 parts per million as a trigger for mass extinction.The term Strangelove ocean is a model name coined by a study published in 1985, which found a decrease in the δ13C values of planktic skeletons following the Cretaceous–Paleogene extinction event, causing a homogenous ocean in decades or centuries, visible in the boundary sediment layer as a manifestation of the elimination in the surface-to-bottom carbon isotope gradient in ocean waters, the halt of ocean primary production. During a time when carbon fractionation by a photosynthesis-respiration mechanism became ineffective. It was later shown that the burial rate of terrestrial organic carbon (biological pump) was likely unaffected.".
- Canfield_ocean wikiPageExternalLink impact-from-the-deep.
- Canfield_ocean wikiPageExternalLink watch?v=HtHlsUDVVy0.
- Canfield_ocean wikiPageID "32661167".
- Canfield_ocean wikiPageLength "4782".
- Canfield_ocean wikiPageOutDegree "20".
- Canfield_ocean wikiPageRevisionID "678454780".
- Canfield_ocean wikiPageWikiLink Anoxic_event.
- Canfield_ocean wikiPageWikiLink Anoxic_waters.
- Canfield_ocean wikiPageWikiLink Biological_pump.
- Canfield_ocean wikiPageWikiLink Category:Geology_theories.
- Canfield_ocean wikiPageWikiLink Cretaceous–Paleogene_extinction_event.
- Canfield_ocean wikiPageWikiLink Donald_Canfield.
- Canfield_ocean wikiPageWikiLink Extinction_event.
- Canfield_ocean wikiPageWikiLink Foraminifera.
- Canfield_ocean wikiPageWikiLink Hydrogen_sulfide.
- Canfield_ocean wikiPageWikiLink Hypoxia_(environmental).
- Canfield_ocean wikiPageWikiLink Mass_extinction.
- Canfield_ocean wikiPageWikiLink Nature_(journal).
- Canfield_ocean wikiPageWikiLink Ocean_anoxia.
- Canfield_ocean wikiPageWikiLink Permian-Triassic_extinction_event.
- Canfield_ocean wikiPageWikiLink Permian–Triassic_extinction_event.
- Canfield_ocean wikiPageWikiLink Peter_Ward_(paleontologist).
- Canfield_ocean wikiPageWikiLink Proterozoic.
- Canfield_ocean wikiPageWikiLink Scientific_American.
- Canfield_ocean wikiPageWikiLink Stratification_(water).
- Canfield_ocean wikiPageWikiLink Suess_effect.
- Canfield_ocean wikiPageWikiLinkText "Canfield ocean".
- Canfield_ocean hasPhotoCollection Canfield_ocean.
- Canfield_ocean wikiPageUsesTemplate Template:Chem.
- Canfield_ocean wikiPageUsesTemplate Template:Cite_journal.
- Canfield_ocean wikiPageUsesTemplate Template:Cite_news.
- Canfield_ocean wikiPageUsesTemplate Template:Geology-stub.
- Canfield_ocean subject Category:Geology_theories.
- Canfield_ocean type Theory.
- Canfield_ocean comment "The Canfield Ocean model refers to the Ocean composition theorized by geologist Donald Canfield. In a seminal paper in Nature in 1998, Canfield argued that the Ocean had become partially anoxic and sulfidic during Proterozoic.Peter Ward studies the effects of ocean hypoxia(anoxic) and sulfidic oceans and climate change.".
- Canfield_ocean label "Canfield ocean".
- Canfield_ocean sameAs m.0h3n47s.
- Canfield_ocean sameAs Q5032319.
- Canfield_ocean sameAs Q5032319.
- Canfield_ocean wasDerivedFrom Canfield_ocean?oldid=678454780.
- Canfield_ocean isPrimaryTopicOf Canfield_ocean.